Bone loss occurs close to a fracture and is associated with increased bone turnover. Fracture healing itself results in increased markers of bone turnover. But the exact patterns of these changes after different fractures are unclear. We aimed to investigate the changes in bone density and biochemical markers following distal forearm fracture. Twenty women (mean age 63 years) were recruited following fracture of the distal radius and ulna. Bone mineral density (BMD) of the hand and forearm were measured by dual-energy X-ray absorptiometry (DXA) and quantitative ultrasound (QUS) of the fingers was measured at 0, 6, 12, 26 and 52 weeks after fracture. Serum and urine samples were collected at 0, 3 and 7 days and at 2, 4, 6, 12, 26 and 52 weeks after fracture to measure markers of bone turnover. For bone formation we measured: bone alkaline phosphatase (iBAP), osteocalcin (Oc), procollagen type I N-terminal propeptide (PINP); and for bone resorption: tartrate-resistant acid phosphatase (TRAcP), free deoxypyridinoline (iFDpd), N-telopeptides of type I collagen (NTx). We used the nonfractured limb to calculate values for baseline BMD and amplitude-dependent speed of sound (AD-SoS). There was a decrease in BMD at the hand and in AD-SoS of the fingers after forearm fracture (p<0.001). This bone loss was maximal for BMD by 6 weeks at 9% (p<0. 001) and remained decreased at 52 weeks. AD-SoS decreased at 12 weeks by 3% (p<0.01) and recovered completely by 52 weeks. Bone formation markers increased between 2 and 4 weeks by 13-52% (p<0. 001), and were still elevated at 52 weeks. Bone resorption markers increased between 2 and 6 weeks by 18-35% and returned to baseline at 52 weeks (TRAcP remained elevated). We conclude that BMD decreased distal and immediately proximal to the fracture line when measured with DXA and QUS. Bone loss after distal forearm fracture did not recover by 52 weeks and most bone turnover markers did not return to baseline.

Bone loss and increased bone turnover are recognized local changes after a fracture, but the exact patterns of these changes after different fractures are unclear. We aimed to investigate the changes in bone density and biochemical markers following ankle fracture. Fourteen subjects (7 postmenopausal women and 7 men, mean age 63 years) were recruited following fracture of the distal tibia and fibula. Bone mineral density (BMD) of the ankle and proximal femur were measured by dual-energy X-ray absorptiometry (DXA) and quantitative ultrasound (QUS) of the calcaneus at 0, 6, 12, 26 and 52 weeks after fracture. Serum and urine samples were collected at 0, 3 and 7 days and at 2, 4, 6, 12, 26 and 52 weeks after fracture to measure markers of bone turnover. For bone formation we measured: bone alkaline phosphatase (iBAP), osteocalcin (Oc), procollagen type I N-terminal propeptide (PINP); and for bone resorption: tartrate-resistant acid phosphatase (TRAcP), deoxypyridinoline (iFDpd), N-telopeptides of type I collagen (NTx). We used the nonfractured limb to calculate values for baseline BMD and QUS. There was a significant decrease in BMD at the ultradistal ankle (p<0.001), the trochanteric region of the hip (p<0.01) and QUS of the heel after ankle fracture. This bone loss was maximal for ultradistal ankle BMD by 6 weeks at 13% (p<0.001) and for the trochanter by 26 weeks at 3% (p<0.01). The ankle BMD returned to baseline at 52 weeks but the trochanter BMD did not. Velocity of sound (VOS) decreased at 6 weeks by 2% (p<0.01) and broadband ultrasound attenuation (BUA) by 15% (p<0.01). VOS recovered completely by 52 weeks, but BUA did not return to baseline. Bone formation markers increased significantly between 1 and 4 weeks by 11-78% (p<0.01), and iBAP returned to baseline at 52 weeks but PINP and Oc remained elevated. Bone resorption markers did not increase and NTx was decreased at 52 weeks. We conclude that BMD decreased distal and immediately proximal to the fracture line when measured with DXA and QUS. Ankle BMD and heel VOS recovered at 52 weeks (trochanteric BMD and heel BUA did not) and the bone turnover markers returned toward baseline.

Background-OV road mountain biking is now an extremely popular recreation and a potent cause of serious injury. Aim-To establish the morbidity associated with this sport. Methods-Data were collected prospectively over one year on all patients presenting with an injury caused by either recreational or competitive oV road mountain biking. Results-Eighty four patients were identified, 70 males and 14 females, with a mean age of 22.5 years (range 8-71). Most accidents occurred during the summer months, most commonly in August. Each patient had an average of 1.6 injuries (n = 133) and these were divided into 15 categories, ranging from minor soft tissue to potentially life threatening. Operative intervention was indicated for 19 patients (23%) and several required multiple procedures. The commonest injuries were clavicle fractures (13%), shoulder injuries (12%), and distal radial fractures (11%). However, of a more sinister nature, one patient had a C2/3 dislocation requiring urgent stabilisation, one required a chest drain for a haemopneumothorax, and another required an emergency and life saving nephrectomy. Conclusion-This sport has recently experienced an explosion in popularity, and, as it carries a significant risk of potentially life threatening injury across all levels of participation, the use of protective equipment to reduce this significant morbidity may be advisable. (Br J Sports Med 2001;35:197-199)

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